Incorporation of marine organic matter by terrestrial detrital food webs: abiotic vs. biotic vectors
2022
Korobushkin, Daniil I. | Saifutdinov, Ruslan A. | Zuev, Andrey G. | Zaitsev, Andrey S.
Marine organic matter can potentially enter terrestrial ecosystems via abiotic or biotic vectors. The former is facilitated by e.g. waves, tides, winds, etc.; the latter – by the activity of organisms, e.g. seabird migration. However, differences in its assimilation rate in detrital food webs at different distance from water remain generally unexplored. To fill this gap, we compared the consumption of marine organics by terrestrial invertebrates within coastal ecosystems of the Black sea using stable isotope analyses of carbon and nitrogen. We focused on relatively inland (100 m from the coast) forested areas with the recently established overwintering colonies of the great cormorant (Phalacrocorax carbo) and control ecosystems isolated from any marine organic matter input. Guano and cormorant food leftover input led to the significant increase of δ¹⁵N values of soil, litter and all trophic groups of soil invertebrates. However, δ¹³C values changed to a smaller extent. The importance of marine resources (in a form of guano) as a carbon source for soil arthropods was relatively low: approximately 15% of their diet. In contrast, coastal soil invertebrates were significantly enriched with ¹³C compared to control and cormorant-influenced ecosystems as they were greatly dependent on the seaweed and other marine resources (on average 45% of coastal invertebrate diet). We conclude that marine resources delivered by an abiotic vector may form the basis of the soil food web diets in a 15 m zone from the water edge. Alternatively, the biotic transfer further inland (forest on a cliff 100 m away from the water edge) with e.g. nitrogen-rich seabird guano or food remains may geographically extend proliferation of marine nutrients into terrestrial ecosystems. As far as we know, our results are among the first to demonstrate the spatial zoning of mechanisms securing bottom-up subsidy of biogenic elements to soil ecosystems having originated from the sea.
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